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  • 1
    Keywords: Earth sciences. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (242 pages)
    Edition: 1st ed.
    ISBN: 9783319138657
    Series Statement: Springer Earth System Sciences Series
    DDC: 363.73874
    Language: English
    Note: Intro -- Acknowledgments -- Contents -- Part I Introduction -- 1 Earth System Science---Past Experiences and Future Trends -- Abstract -- 1 Introduction -- 2 Review -- 3 Future Trends -- 4 Conclusion -- References -- 2 The Educational Program of the Earth System Science Research School (ESSReS) -- Abstract -- 1 Introduction -- 2 The Educational Program -- 2.1 Introductory Courses -- 2.2 Expert Courses -- 2.3 Seminar Series -- 2.4 Computational Skills Courses -- 2.5 Transferable Skill Courses -- 2.6 Academic Writing Courses -- 2.7 Excursions -- 2.8 Annual Retreat -- 3 International Exchange -- 3.1 International and National Meetings -- 3.2 Visit in a Foreign Lab -- 3.3 Invited Guest Scientists -- 4 Progress Assessments -- 5 Conclusions -- References -- 3 Time Evolution of a PhD Student's Mood---A Review of My Time as PhD Student of the Research School ESSReS -- 1 Introduction -- 2 Time Evolution of a PhD Students's Mood -- 3 Conclusion -- References -- 4 Progress in Earth System Science: What Does It Take to Make Our Ideas Clear? -- Abstract -- 1 Self-critical Approach -- 2 Hypothesis Testing and Models -- 3 Building of Models and Expressing the Scientific Discoveries -- References -- Part II Remote Sensing and Modelling of Atmospheric Chemistry and Sea Ice Parameters -- 5 Towards a Better Tropospheric Ozone Data Product from SCIAMACHY: Improvements in High Latitude Stratospheric Ozone -- Abstract -- 1 Introduction -- 2 Limb Measurements and Comparison Methodology -- 3 SCIAMACHY Limb Retrieval of Version 2.9 -- 4 SCIAMACHY Limb Retrieval of Version 3.0 and Comparison Results -- 5 Conclusions -- Acknowledgments -- References -- 6 Ten-Year SCIAMACHY Stratospheric Aerosol Data Record: Signature of the Secondary Meridional Circulation Associated with the Quasi-Biennial Oscillation -- Abstract -- 1 Introduction -- 2 Instrument and Data. , 3 Results and Discussion -- 4 Conclusions -- Acknowledgments -- References -- 7 Investigating the Link Between Glyoxal and Biogenic Activities -- Abstract -- 1 Introduction -- 2 Glyoxal Retrieval -- 3 Results and Discussion -- 4 Conclusions -- Acknowledgments -- References -- 8 Estimates of NOx Emission Factors from GOME-2 Measurements for the Major Types of Open Biomass Burning -- Abstract -- 1 Introduction -- 2 Data and Methods -- 2.1 Satellite Measurements of TVC NO2 -- 2.2 Satellite Measurements of FRP -- 2.3 Land Cover Type Product -- 2.4 Production Rate of NOx from Fire -- 2.5 Estimation of NOx Emission Factors -- 3 Results and Discussion -- 4 Conclusions and Outlook -- References -- 9 The Use of FTIR-Spectrometry in Combination with Different Biosphere-Atmosphere Flux Measurement Techniques -- Abstract -- 1 Introduction -- 2 Experimental Setup -- 2.1 The Flux Gradient Technique -- 2.2 The Flux Chamber Technique -- 3 Flux Gradient- and Flux Chamber Measurements -- 4 Discussion and Conclusion -- Acknowledgments -- References -- 10 Near-Infrared Lunar Absorption Spectroscopy for the Retrieval of Column Averaged CO2 and CH4 -- Abstract -- 1 Introduction -- 2 Ground-Based Column Averaged Trace Gas Retrieval -- 3 Spectra from the Bremen Instrument Setup -- 4 xCO2 and xCH4 from Lunar Absorption Spectroscopy -- 5 Conclusions -- Acknowledgements -- References -- 11 A New Method to Filter Out Radio-Frequency Interference (RFI) from SMOS Level 1C Data for Sea Ice Applications -- Abstract -- 1 Introduction -- 2 Data Description -- 3 Filtering Procedure -- 4 Conclusion -- Acknowledgments -- References -- 12 Arctic Multiyear Ice Concentration Retrieval from SSM/I Data Using the NASA Team Algorithm with Dynamic Tie Points -- Abstract -- 1 Introduction -- 2 Method -- 3 Time Series Results -- 4 Sensitivity Study and Conclusion -- Acknowledgements -- References. , 13 Detecting CDOM Fluorescence Using High Spectrally Resolved Satellite Data: A Model Study -- Abstract -- 1 Introduction -- 2 Methods -- 2.1 DOAS Retrieval Technique -- 2.2 CDOM Fluorescence Modeling -- 2.2.1 CDOM as Mixture of Humic and Fulvic Acids -- 2.2.2 Excitation-Emission Matrices Approach -- 3 Results and Discussion -- 4 Conclusions and Outlook -- Acknowledgments -- References -- Part III Physical Oceanography -- 14 The Flow of Dense Water Plumes in the Western Weddell Sea Simulated with the Finite Element Ocean Model (FEOM) -- Abstract -- 1 Introduction -- 2 Model Setup and Experiments -- 3 Results -- 4 Summary and Conclusions -- Acknowledgments -- References -- 15 Data Analysis and Modeling of the Amundsen Sea Embayment -- Abstract -- 1 Introduction -- 2 Hydrographic Data Analysis -- 3 Modeling of the Amundsen Sea -- 4 Discussion and Outlook -- References -- Part IV Sea-ice Physics -- 16 Impact of Sea-Ice Bottom Topography on the Ekman Pumping -- Abstract -- 1 Introduction -- 2 Data and Methods -- 3 Calculation of Oceanic Drag Coefficients -- 4 Ekman Pumping -- 5 Summary and Conclusion -- Acknowledgments -- References -- 17 Classification of CryoSat-2 Radar Echoes -- Abstract -- 1 Introduction -- 2 Methods -- 3 Results -- 4 Discussion -- 5 Conclusion -- Acknowledgments -- References -- Part V Earth System Modelling and Data Analysis -- 18 Integration of Passive Tracers in a Three-Dimensional Ice Sheet Model -- Abstract -- 1 Introduction -- 2 Methods -- 2.1 Present Day Control Run -- 2.2 Passive Tracer Advection -- 2.2.1 Validation of Tracer Modules -- 2.2.2 Analytical Comparison to the Nye-Vialov Solution -- 3 Discussion -- References -- Part VI Climate Archives and Geotectonics -- 19 Bivalve Shells---Unique High-Resolution Archives of the Environmental Past -- Abstract -- 1 Introduction -- 2 Methods -- 2.1 Shell Origin and Laboratory Work. , 2.2 State of Preservation -- 2.3 Frequency Analysis -- 2.4 Stable Oxygen Isotopes ( delta 18O) -- 3 Results -- 3.1 State of Preservation -- 3.2 Frequency Analysis -- 3.3 Stable Oxygen Isotopes ( delta 18O) -- 4 Discussion and Conclusions -- Acknowledgments -- References -- 20 Functional Diversity and Traits Assembly Patterns of Benthic Macrofaunal Communities in the Southern North Sea -- Abstract -- 1 Introduction -- 2 Material and Methods -- 3 Results -- 4 Discussion -- Acknowledgments -- 21 Snow Accumulation in North Greenland over the Last Millennium -- Abstract -- 1 Introduction -- 2 Methods -- 3 Results -- 4 Discussion and Conclusion -- References -- 22 Seismostratigraphic Analysis and Glacial History of the Weddell Sea Region, Antarctica -- Abstract -- 1 Introduction -- 2 Data and Methods -- 3 Results -- 3.1 Seismic Characteristics and Horizon Stratigraphy -- 3.2 Sedimentation Rates -- 4 Discussion and Conclusions -- Acknowledgments -- References -- Part VII Geoinformatics -- 23 Visual Analysis of Relevant Fields in Geoscientific Multifield Data -- Abstract -- 1 Introduction -- 2 Related Work -- 3 Field Similarity Plot -- 4 Interactive Visual Analysis -- 5 Use Cases -- 5.1 Multifield -- 5.2 Time-Varying Field -- 6 Discussion -- 7 Conclusion -- Acknowledgements -- References -- 24 A Database Language More Suitable for the Earth System Sciences -- Abstract -- 1 Introduction -- 2 Data Model -- 3 Query Language -- 3.1 Array Construction -- 3.2 Array Inspection Operators -- 3.3 Array Aggregation -- 3.4 Derived Operators -- 3.5 Array \leftrightarrow Table Conversion -- 3.6 Array \leftrightarrow LOB Conversion -- 4 Implementation -- 5 Conclusion -- Acknowledgments -- References -- 25 Towards Collaborative Exploration and Analysis of Big Data from Mars: A Noachis Terra Case Study -- Abstract -- 1 Introduction -- 2 Data and Methods. , 3 Noachis Terra Case Study -- 4 Discussion -- 5 Conclusions -- Acknowledgments -- References.
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  • 2
    Keywords: Earth System Sciences ; Physical geography. ; Atmospheric sciences. ; Geography
    Description / Table of Contents: 1 Earth System Science - past experiences and future trends -- 2 The educational program of the Earth System Science Research School (ESSReS) -- 3 Time evolution of a PhD student's mood - A review of my time as PhD student in the research school ESSReS -- 4 Progress in Earth System Science: What does it take to make our ideas clear -- 5 Towards a better tropospheric ozone product from SCIAMACHY: improvements in high latitude stratospheric ozone -- 6 Ten-year SCIAMACHY Stratospheric Aerosol data record: Signature of the Secondary Meridional Circulation associated with the Quasi-Biennial Oscillation in the Tropical Stratosphere -- 7 Investigating the link between glyoxal and biogenic activities -- 8 Estimates of NOx emission factors from GOME-2 measurements for the major types of open biomass burning -- 9 The use of FTIR-spectrometry in combination with different biosphere-atmosphere flux measurement techniques -- 10 Near-infrared lunar absorption spectroscopy for the retrieval of column averaged CO2 and CH4 -- 11 A new method to filter out radio-frequency interference (RFI) from SMOS level 1C data for sea ice applications -- 12 Arctic Multiyear Ice Concentration Retrieval from SSM/I data using the NASA Team algorithm with dynamic tie points -- 13 Detecting CDOM fluorescence using high spectrally resolved satellite data: a model study -- 14 The flow of dense water plumes in the western Weddell Sea simulated with the Finite Element Ocean Model (FEOM) -- 15 Data analysis and modeling of the Amundsen Sea embayment -- 16 Impact of sea-ice bottom topography on the Ekman pumping -- 17 Classification of CryoSat-2 radar echoes -- 18 Integration of passive tracers in a three-dimensional ice sheet model -- 19 Bivalve shells - unique high-resolution archives of environmental past -- 20 Functional diversity and traits assembly patterns of benthic macrofaunal communities in the southern North Sea -- 21 Snow accumulation in North Greenland over the last millennium -- 22 Seismostratigraphic analysis and glacial history of the Weddell Sea region, Antarctica -- 23 Visual analysis of Relevant Fields in Geoscientific Multifield Data -- 24 A Database Language Suitable for the Earth System Sciences -- 25 Towards Collaborative Exploration and Analysis of Big Data from Mars: A Noachis Terra Case Study
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (X, 251 p. 86 illus., 83 illus. in color)
    Edition: 1st ed. 2015
    ISBN: 9783319138657
    Series Statement: Springer Earth System Sciences
    Language: English
    Note: Description based upon print version of record , 1 Earth System Science - past experiences and future trends2 The educational program of the Earth System Science Research School (ESSReS) -- 3 Time evolution of a PhD student's mood - A review of my time as PhD student in the research school ESSReS -- 4 Progress in Earth System Science: What does it take to make our ideas clear -- 5 Towards a better tropospheric ozone product from SCIAMACHY: improvements in high latitude stratospheric ozone -- 6 Ten-year SCIAMACHY Stratospheric Aerosol data record: Signature of the Secondary Meridional Circulation associated with the Quasi-Biennial Oscillation in the Tropical Stratosphere -- 7 Investigating the link between glyoxal and biogenic activities -- 8 Estimates of NOx emission factors from GOME-2 measurements for the major types of open biomass burning -- 9 The use of FTIR-spectrometry in combination with different biosphere-atmosphere flux measurement techniques -- 10 Near-infrared lunar absorption spectroscopy for the retrieval of column averaged CO2 and CH4 -- 11 A new method to filter out radio-frequency interference (RFI) from SMOS level 1C data for sea ice applications -- 12 Arctic Multiyear Ice Concentration Retrieval from SSM/I data using the NASA Team algorithm with dynamic tie points -- 13 Detecting CDOM fluorescence using high spectrally resolved satellite data: a model study -- 14 The flow of dense water plumes in the western Weddell Sea simulated with the Finite Element Ocean Model (FEOM) -- 15 Data analysis and modeling of the Amundsen Sea embayment -- 16 Impact of sea-ice bottom topography on the Ekman pumping -- 17 Classification of CryoSat-2 radar echoes -- 18 Integration of passive tracers in a three-dimensional ice sheet model -- 19 Bivalve shells - unique high-resolution archives of environmental past -- 20 Functional diversity and traits assembly patterns of benthic macrofaunal communities in the southern North Sea -- 21 Snow accumulation in North Greenland over the last millennium -- 22 Seismostratigraphic analysis and glacial history of the Weddell Sea region, Antarctica -- 23 Visual analysis of Relevant Fields in Geoscientific Multifield Data -- 24 A Database Language Suitable for the Earth System Sciences -- 25 Towards Collaborative Exploration and Analysis of Big Data from Mars: A Noachis Terra Case Study.
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  • 3
    Publication Date: 2020-08-07
    Description: NW African climate shows orbital and millennial-scale variations, which are tightly connected to changes in marine productivity. We present an organic-walled dinoflagellate cyst (dinocyst) record from a sediment core off Cape Yubi at about 27°N in the Canary Basin covering the time period from 47 to 3 ka before present (BP). The dinocyst record reflects differences in upwelling intensity and seasonality as well as the influence of fluvial input. Sea-level changes play an important role for the upwelling pattern and productivity signals at the core site. Within the studied time interval, four main phases were distinguished. (1) From 45 to 24 ka BP, when sea-level was mostly about 75 m lower than today, high relative abundances of cysts of heterotrophic taxa point to enhanced upwelling activity, especially during Heinrich Events, while relatively low dinocyst accumulation rates indicate that filament activity at the core location was strongly reduced. (2) At sea-level lowstand during the LGM to H1, dinocyst accumulation rates suggest that local filament formation was even more inhibited. (3) From the early Holocene to about 8 ka BP, extraordinary high accumulation rates of most dinocyst species, especially of Lingulodinium machaerophorum, suggest that nutrient supply via fluvial input increased and rising sea-level promoted filament formation. At the same time, the upwelling season prolongated. (4) A relative increase in cysts of photoautotrophic taxa from about 8 ka BP onwards indicates more stratified conditions while fluvial input decreased. Our study shows that productivity records can be very sensitive to regional features. From the dinocyst data we infer that marine surface productivity off Cape Yubi during glacial times was within the scale of modern times but extremely enhanced during deglaciation.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2014-05-12
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
    Format: application/pdf
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  • 5
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2005. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 20 (2005): PA1016, doi:10.1029/2004PA001103.
    Description: Radiocarbon age relationships between co-occurring planktic foraminifera, alkenones and total organic carbon in sediments from the continental margins of Southern Chile, Northwest Africa and the South China Sea were compared with published results from the Namibian margin. Age relationships between the sediment components are site-specific and relatively constant over time. Similar to the Namibian slope, where alkenones have been reported to be 1000 to 4500 years older than co-occurring foraminifera, alkenones were significantly (~1000 yrs) older than co-occurring foraminifera in the Chilean margin sediments. In contrast, alkenones and foraminifera were of similar age (within 2σ error or better) in the NW African and South China Sea sediments. Total-organic-matter and alkenone ages were similar off Namibia (age difference TOC-alkenones: 200-700 years), Chile (100-450 years), and NW Africa (360-770 years), suggesting minor contributions of pre-aged terrigenous material. In the South China Sea total organic carbon is significantly (2000-3000 yrs) older due to greater inputs of pre-aged terrigenous material. Age offsets between alkenones and planktic foraminifera are attributed to lateral advection of organic matter. Physical characteristics of the depositional setting, such as sea-floor morphology, shelf width, and sediment composition, may control the age of co-occurring 2 sediment components. In particular, offsets between alkenones and foraminifera appear to be greatest in deposition centers in morphologic depressions. Aging of organic matter is promoted by transport. Age offsets are correlated with organic richness, suggesting that formation of organic aggregate is a key process.
    Description: GM and MK acknowledge financial support from the WHOI postdoctoral scholarship program. This work was funded by NSF grant OCE-0327405.
    Keywords: Compound-specific radiocarbon dating ; Alkenones ; High accumulation rate sediments
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 6
    Publication Date: 2019-08-19
    Description: Post-graduate education in Germany has changed a lot over the past decades. Formerly, PhD students generally did not have the option to attend formal classes and lectures and were expected to conduct their independent research, including occasionally teaching courses for students. Since the introduction of bachelor and masters studies with the Bologna Process in the late 90th, the higher education in Europe has been harmonized, leading to more structured and focused studies at the expense of a broad and universal disciplinary education. At this same time, special fields such as Earth System Science became more interdisciplinary. In consequence, universities and research institutes have established so-called research schools and/or graduate schools, offering specific courses and training alongside the doctorate. Especially, Earth System Science has developed from an interesting concept in Earth Sciences education to a fully integrative Science focussed on understanding the complex system Earth. This evolution is partially due to the radical and far reaching anthropogenic changes and the general feeling of helplessness with regards to the possible consequences and future impacts on the Earth System. The Helmholtz “Earth System Science Research School” (ESSReS) is a small unit of PhD students co-organized by three educational and research institutions in the city state Bremen: University of Bremen (Institute for Environmental Physics, IUP), Jacobs University (School of Engineering and Science (JU)), and Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research in Bremerhaven (AWI). ESSReS aims at the integration of research at the interface of Geology, Biology, Physics, Geophysics, Mathematics and Informatics. It is therefore multi- and interdisciplinary in every aspect. The training, curriculum, and PhD research subjects are closely located at the interfaces between the participating disciplines. This is guaranteed by interdisciplinary supervision of the PhD project. The long-term goal of ESSReS is not only to enhance exchange and interaction between these disciplines, but to enforce a newly integrated concept, where separation between disciplines becomes more and more obsolete. Now, at the end of two three-years terms of PhD student education it can be stated that ESSReS provide a solid base for a new generation of excellent scientists in Earth and Environmental Sciences.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
    Format: application/pdf
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  • 7
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    Springer
    In:  EPIC3Towards an Interdisciplinary Approach in Earth System Science, Earth System Science—Past Experiences and Future Trends, Heidelberg, Springer, pp. 3-7, ISBN: 978-3-319-13864-0, ISSN: 2197-9596
    Publication Date: 2023-06-21
    Description: Earth System Science has developed over the last two decades from an interesting concept in Earth sciences education to a fully integrative science focussed on understanding the complex system Earth. This evolution is partially due to the radical and far reaching anthropogenic changes and the general feeling of helplessness with regards to the possible consequences and future impacts on the Earth System. This paper proposes that a paradigm shift in undergraduate and graduate education is needed to further develop Earth System Science. Graduate programs such as the Earth System Science Research School (ESSReS), which are intrinsically trans- and interdisciplinary will help to change rigid subject specific mind-set among faculty and students. The health and sustainability of our planet is at stake
    Repository Name: EPIC Alfred Wegener Institut
    Type: Inbook , peerRev
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  • 8
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    Springer
    In:  EPIC3Towards an Interdisciplinary Approach in Earth System Science, Towards an Interdisciplinary Approach in Earth System Science, Heidelberg, Springer, pp. 9-17, ISBN: 978-3-319-13864-0
    Publication Date: 2023-06-21
    Description: The Earth System Science Research School (ESSReS) is an international and interdisciplinary research school for 23 PhD students at the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research (AWI) and their partner universities: University of Bremen and Jacobs University Bremen. ESSReS combines observations, modelling, and data analysis in order to decipher the Earth’s complex climate system. Structured training, international exchange and supervision support interdisciplinary research at an early stage of the scientific career.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Inbook , peerRev
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  • 9
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    PANGAEA
    In:  Supplement to: Kuhnert, Henning; Kuhlmann, Holger; Mohtadi, Mahyar; Meggers, Helge; Baumann, Karl-Heinz; Pätzold, Jürgen (2014): Holocene tropical western Indian Ocean sea surface temperatures in covariation with climatic changes in the Indonesian region. Paleoceanography, https://doi.org/10.1002/2013PA002555
    Publication Date: 2023-03-03
    Description: The sea surface temperature (SST) of the tropical Indian Ocean is a major component of global climate teleconnections. While the Holocene SST history is documented for regions affected by the Indian and Arabian monsoons, data from the near-equatorial western Indian Ocean are sparse. Reconstructing past zonal and meridional SST gradients requires additional information on past temperatures from the western boundary current region. We present a unique record of Holocene SST and thermocline depth variations in the tropical western Indian Ocean as documented in foraminiferal Mg/Ca ratios and d18O from a sediment core off northern Tanzania. For Mg/Ca and thermocline d18O, most variance is concentrated in the centennial to bicentennial periodicity band. On the millennial time scale, an early to mid-Holocene (~7.8-5.6 ka) warm phase is followed by a temperature drop by up to 2°C, leading to a mid-Holocene cool interval (5.6-4.2 ka). The shift is accompanied by an initial reduction in the difference between surface and thermocline foraminiferal d18O, consistent with the thickening of the mixed layer and suggestions of a strengthened Walker circulation. However, we cannot confirm the expected enhanced zonal SST gradient, as the cooling of similar magnitude had previously been found in SSTs from the upwelling region off Sumatra and in Flores air temperatures. The SST pattern probably reflects the tropical Indian Ocean expression of a large-scale climate anomaly rather than a positive Indian Ocean Dipole-like mean state.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 10
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    PANGAEA
    In:  Supplement to: Freudenthal, Tim; Neuer, Susanne; Meggers, Helge; Davenport, Robert; Wefer, Gerold (2001): Influence of lateral particle advection and organic matter degradation on sediment accumulation and stable nitrogen isotope ratios along a productivity gradient in the Canary Islands region. Marine Geology, 177(1-2), 93-109, https://doi.org/10.1016/S0025-3227(01)00126-8
    Publication Date: 2023-05-12
    Description: We compare total and biogenic particle fluxes and stable nitrogen isotope ratios (d15N) at three mooring sites along a productivity gradient in the Canary Islands region with surface sediment accumulation rates and sedimentary d15N. Higher particle fluxes and sediment accumulation rates, and lower d15N were observed in the upwelling influenced eastern boundary region (EBC) compared to the oligotrophic sites north of Gran Canaria [European Station for Time-Series in the Ocean, Canary Islands (ESTOC]] and north of La Palma (LP). The impact of organic matter degradation and lateral particle advection on sediment accumulation was quantified with respect to the multi-year flux record at the ESTOC. Remineralisation of organic matter in the water column and at the sediment surface resulted in an organic carbon preservation of about 0.8% and total nitrogen preservation of about 0.4% of the estimated export production. Higher total and carbonate fluxes and accumulation rates in the lower traps and surface sediment compared to the upper traps indicated that at least 50% of the particulate matter at the ESTOC was derived from allochthonous sources. Low d15N values in the lower traps of the ESTOC and LP point to a source region influenced by coastal upwelling. We conclude from this study that the reconstruction of export production or nutrient regimes from sedimentary records in regions with strong productivity gradients might be biased due to the mixture of particles originating from autochthonous and allochthonous sources. This could result in an imprint of high productivity signatures on sedimentation processes in oligotrophic regions.
    Keywords: Canary Islands Azores Gibraltar Observations; CANIGO; ESTOC; European Station for Time-Series in the Ocean Canary Islands; GeoB; Geosciences, University of Bremen
    Type: Dataset
    Format: application/zip, 4 datasets
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